When polar air dipping southward collides with
rising warm tropical air, the meet - up causes a powerful atmospheric wave with rollercoaster - like patterns that propagate eastward around the globe.
Not exact matches
The Walker circulation refers to the mean (steady) ciculation where
air over the
warm pool in the western part of the
tropical Pacific
rises, being fed by the easterly surface trade winds across the Pacific, and subsidence over eastern Pacific.
Normally in the
tropical Pacific, a major area of
rising air is found over the western portions, where the
warmest waters are found.
All of these ingredients —
warm water, westerly winds, and
rising air — have made for a very favorable
tropical cyclone environment.
All that extra heat in the
tropical Pacific Ocean
warms up the atmosphere above it, leading to more
rising air, which changes the circulation all around the globe.
As the
air rises, it expands and cools, and water vapour condenses, releasing even more heat,» much like how a hurricane frees energy by drawing
warm humid
air from its base (usually
tropical sea water) and then releasing cold, wet
air 7 miles (12 kilometers) up in the troposphere.
Hurricanes (Fig. 7) and other
tropical cyclones can be thought of as heat engines that take energy in by evaporating
warm ocean water, and eject it at a colder temperature near the tropopause after
air rises and water condenses in the eyewall [14].
This somewhat migratory zone was the Silurian intertropical convergence zone (ITCZ), where the convergence of Northern and Southern Hemispheric trade winds caused the
warm tropical air to
rise, which in turn produced regular cloud cover and precipitation.